
metamorphic
Coarse-grained metamorphic rock, likely amphibolite or hornblende gneiss
Amphibolite; predominantly hornblende amphibole and plagioclase feldspar, possibly with quartz and biotite
AI-generated identification · may be incorrectDark gray-green, speckled, granular and weakly foliated, with dull to slightly vitreous luster; amphibole hardness ~5–6 and feldspar ~6, with no obvious cleavage visible at this resolution. Specific gravity is commonly about 2.9–3.2.
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Physical properties
Dark gray-green, speckled, granular and weakly foliated, with dull to slightly vitreous luster; amphibole hardness ~5–6 and feldspar ~6, with no obvious cleavage visible at this resolution. Specific gravity is commonly about 2.9–3.2.
Formation & geological history
Formed when basaltic or gabbroic rock underwent medium- to high-grade regional metamorphism, commonly during Precambrian to younger mountain-building events. The exact age cannot be determined from the photograph.
Uses & applications
Used locally as crushed aggregate, road stone, riprap, and dimension stone; attractive polished pieces may be sold as decorative specimens, but it is not generally a gemstone.
Geological facts
Amphibolite’s green-black color reflects abundant hornblende, while lighter grains are commonly plagioclase. Strong alignment of amphibole crystals may produce a gneissic or schistose texture.
Field identification & locations
Look for a dense greenish-black rock with interlocking crystals, amphibole splinters, and possible foliation; a streak, hardness, and thin-section test would improve identification. Common in metamorphic belts worldwide, including the Appalachians, Canadian Shield, and Scandinavia.
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